Resiliencia climática en las zonas desérticas de Egipto
DOI:
https://doi.org/10.35305/cl.vi22.135Palabras clave:
Egipto, desierto, adaptación, cambio climático, precipitacionesResumen
Hoy en día, la región del Sahara es conocida como un entorno hiperárido con una mínima actividad humana por fuera de los pocos oasis. Sin embargo, la evidencia arqueológica sugiere que, en el pasado, el paisaje era más accesible y que los asentamientos surgieron alrededor de manantiales y pozos que estaban conectados por rutas muy transitadas. Nuestros estudios sugieren que la actividad se concentró en períodos históricos en los que había agua dulce disponible particularmente en la Dinastía XVIII durante el Reino Nuevo y en el período greco-romano. La comparación con los registros de indicadores de temperatura global en el “Greenland Ice Sheet Project” (Proyecto Inlandsis) muestra que estos períodos de actividad también fueron épocas de altas temperaturas globales, lo que lleva a la conclusión de que los períodos de calentamiento global producen un aumento de las precipitaciones en la región del Sahara que sustentan los ecosistemas y la actividad en el desierto.
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